{
    "created": "2022-09-08 10:55:01",
    "updated": "2026-05-06 06:27:29",
    "id": "97bec087-1e45-4e92-a83b-623b2e4b4be8",
    "version": 5,
    "ds_topic": null,
    "title_cn": "柴达木地区100km分辨率0℃层高度变化数据集（1985-2018年）",
    "title_en": "Data set of height change of 0 ℃ layer with 100km resolution in Qaidam area (1985-2018)",
    "ds_abstract": "<p>&emsp;&emsp;0℃层高度是大气探测的一个重要特性层，反映着大气对流层中下层的温度状况，该层的升降一定程度上影响山体地表：0℃线的升降，进而影响山区水的冻融过程。分析中国西部39个高空观测站从1979年以来（部分观测站观测时间较晚）的高空站规定层高度和温度，计算夏季(6-8月) 0℃层的高度，进行Kriging插值、回归分析等方法计算得到1985-2018年柴达木盆地夏季0℃层的变化，通过渔网工具，统计每100km 0℃层高度变化。",
    "ds_source": "<p>&emsp;&emsp;原始数据为中国高空气象站观测资料。包含了国家气象信息中心通过国内通信系统获取的89个中国探空观测站点各规定等压面和压温湿特性层位势高度、温度、露点温度、风向、风速观测数据。",
    "ds_process_way": "<p>&emsp;&emsp;分析中国西部39个高空站规定层的高度和温度，计算夏季(6-8月) 0℃层的高度，以100km空间分辨率进行Kriging插值、回归分析等方法计算得到1985-2018年柴达木盆地夏季0℃层的变化，通过渔网工具，统计每100km 0℃层高度变化。",
    "ds_quality": "<p>&emsp;&emsp;数据质量良好。",
    "ds_acq_start_time": "1985-01-01 00:00:00",
    "ds_acq_end_time": "2018-12-31 00:00:00",
    "ds_acq_place": "柴达木盆地",
    "ds_acq_lon_east": 99.25,
    "ds_acq_lat_south": 35.0,
    "ds_acq_lon_west": 90.25,
    "ds_acq_lat_north": 39.31666666666667,
    "ds_acq_alt_low": null,
    "ds_acq_alt_high": null,
    "ds_share_type": "login-access",
    "ds_total_size": 71729,
    "ds_files_count": 2,
    "ds_format": "tif ",
    "ds_space_res": "100km",
    "ds_time_res": "",
    "ds_coordinate": "WGS84",
    "ds_projection": "",
    "ds_thumbnail": "97bec087-1e45-4e92-a83b-623b2e4b4be8.jpg",
    "ds_thumb_from": 0,
    "ds_ref_way": "",
    "paper_ref_way": "",
    "ds_ref_instruction": "",
    "ds_from_station": null,
    "organization_id": "4851e874-eafc-4879-812b-ffbdd825e967",
    "ds_serv_man": "敏玉芳",
    "ds_serv_phone": "0931-4967596",
    "ds_serv_mail": "ncdc@lzb.ac.cn",
    "doi_value": "10.12072/ncdc.Hydro.db2423.2022",
    "subject_codes": [
        "170.45"
    ],
    "quality_level": 3,
    "publish_time": "2022-09-29 11:02:43",
    "last_updated": "2025-04-29 15:29:55",
    "protected": false,
    "protected_to": null,
    "lang": "zh",
    "cstr": "11738.11.ncdc.Hydro.db2423.2022",
    "i18n": {
        "en": {
            "title": "Data set of height change of 0 ℃ layer with 100km resolution in Qaidam area (1985-2018)",
            "ds_format": "TIF",
            "ds_source": "<p>&emsp; The raw data were obtained from China's upper-air meteorological station observations, comprising upper-air measurements from 89 radiosonde stations across China. These data were acquired by the National Meteorological Information Center (NMIC) through the domestic meteorological telecommunication system and include the following variables at standard pressure levels and significant levels: geopotential height, temperature, dew-point temperature, wind direction, and wind speed.",
            "ds_quality": "<p>&emsp; The data quality is good.",
            "ds_ref_way": "",
            "ds_abstract": "<p> The 0°C isotherm height is a significant characteristic layer in atmospheric sounding, reflecting the thermal conditions of the middle and lower troposphere. The rise and fall of this layer influence the surface elevation of the 0°C isotherm in mountainous regions, thereby affecting the freeze-thaw processes of water in these areas.By analyzing upper-air data from 39 high-altitude observation stations in western China since 1979 (with some stations having later observation records), including standard-level heights and temperatures, the summer (June-August) 0°C isotherm height was calculated. Using Kriging interpolation and regression analysis, the variation of the summer 0°C isotherm height in the Qaidam Basin from 1985 to 2018 was derived. Additionally, a fishnet tool was employed to statistically assess the 0°C isotherm height change per 100 km grid.</p>",
            "ds_time_res": "",
            "ds_acq_place": "Qaidam Basin",
            "ds_space_res": "100km",
            "ds_projection": "",
            "ds_process_way": "<p>&emsp;&emsp;Using geopotential height and temperature data from standard pressure levels at 39 upper-air stations in western China, we calculated the summer (June-August) 0°C isotherm height. Through Kriging interpolation and regression analysis at 1 km spatial resolution, we derived the variations of summer 0°C isotherm over the Qaidam Basin during 1985-2018. A fishnet grid analysis was employed to quantify altitude changes of the 0°C isotherm per 1 km grid cell.",
            "ds_ref_instruction": ""
        }
    },
    "submit_center_id": "ncdc",
    "data_level": 0,
    "license_type": "CC BY 4.0",
    "doi_reg_from": "reg_local",
    "cstr_reg_from": "reg_local",
    "doi_not_reg_reason": null,
    "cstr_not_reg_reason": null,
    "is_paper_in_submitting": false,
    "ds_topic_tags": [
        "柴达木盆地",
        "0℃层高度变化",
        "100km"
    ],
    "ds_subject_tags": [
        "地理学"
    ],
    "ds_class_tags": [],
    "ds_locus_tags": [
        "柴达木盆地"
    ],
    "ds_time_tags": [
        1985,
        1986,
        1987,
        1988,
        1989,
        1990,
        1991,
        1992,
        1993,
        1994,
        1995,
        1996,
        1997,
        1998,
        1999,
        2000,
        2001,
        2002,
        2003,
        2004,
        2005,
        2006,
        2007,
        2008,
        2009,
        2010,
        2011,
        2012,
        2013,
        2014,
        2015,
        2016,
        2017,
        2018
    ],
    "ds_contributors": [
        {
            "true_name": "朱高峰",
            "email": "zhugf@lzu.edu.cn",
            "work_for": "兰州大学",
            "country": "中国"
        }
    ],
    "ds_meta_authors": [
        {
            "true_name": "石梦寒",
            "email": "shimh20@lzu.edu.cn",
            "work_for": "兰州大学",
            "country": "中国"
        }
    ],
    "ds_managers": [
        {
            "true_name": "朱高峰",
            "email": "zhugf@lzu.edu.cn",
            "work_for": "兰州大学",
            "country": "中国"
        }
    ],
    "category": "气象"
}